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Q: Which is not an example of a small crustal fragment that could collide with a continental landmass forming mountainous topography?
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Related questions

Which continental Landmass has no countries?

Antarctica


What is the Steep boundary between the continental landmass and the ocean basin?

the answer to the question is: continental slope


Who study movements of continental landmass?

Geologists study the movements of continental landmasses through the field of plate tectonics. They investigate how the Earth's lithosphere is broken into plates that move over the semi-fluid asthenosphere, leading to phenomena such as earthquakes, mountain building, and the formation of ocean basins.


What is the continental edge?

The continental shelf edge is an area that is located at the edge of an underwater landmass. This landmass extends out from a continent and has a relatively shallow area of water which is often referred to as the shelf sea.


What island is Europe on?

Europe is not on an island. It is part of the continental landmass known as Eurasia.


What is Europe's islands?

Europe is not on an island. It is part of the continental landmass known as Eurasia.


What is the idea that all continents were all one big landmass?

a continental theory


Idea that all continents were once a single landmass but are now separate is called?

This idea is called the theory of continental drift, which suggests that all continents were once part of a single landmass called Pangaea that later split and drifted apart over millions of years.


What is the name of landmass Alfred wegener?

Alfred wegener came up with the theory of continental drift, when all of the continents were together as one the landmass was called Pangea


Is the continent of Europe an island?

No. It is joined to Asia, forming a continental landmass known as Eurasia.


What is the idea that all continets were part of one big landmass?

continental drift :D


Does sediment build up at the continental shelf?

The continental shelves were formed millions of years ago, when most of the land on the Earth was compacted into one huge landmass. After some time, this landmass began to break into smaller pieces, which became the continental shelves. Then they drifted farther and farther apart and appear where they are today.